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The warmer ocean water that flows south from the tropics mostly affects the ice shelves around the Antarctic Peninsula.

The Antarctic Bottom Water -- a natural phenomenon produced by the extreme cold -- is the most dense of all ocean waters, given its high saline content: 34.65%. Because warm water weighs less than cold water, the surface waters flow over the colder, more dense water.

Wherever the warmer water flows under the ice shelves, these shelves are beginning to disintegrate from below.

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9y ago

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